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红壤丘陵区旱地和水旱轮作地土壤中纤维素降解功能微生物群落特征
引用本文:王雨晴,陈香碧,董明哲,冯书珍,胡亚军,苏以荣,葛体达,张振华,李巧云.红壤丘陵区旱地和水旱轮作地土壤中纤维素降解功能微生物群落特征[J].农业环境科学学报,2017,36(10):2071-2079.
作者姓名:王雨晴  陈香碧  董明哲  冯书珍  胡亚军  苏以荣  葛体达  张振华  李巧云
作者单位:湖南农业大学生物科技学院, 长沙 410128;中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125;广西科技大学, 广西 柳州 545006,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,中国科学院亚热带农业生态研究所, 亚热带农业生态重点实验室, 长沙 410125,湖南农业大学南方粮油作物协同创新中心, 长沙 410128,湖南农业大学生物科技学院, 长沙 410128
基金项目:国家重点研发计划项目(2016YFD0200106-5);国家自然科学基金项目(41671298,41301273);"西部之光"人才培养计划
摘    要:为揭示农田土壤有机质中纤维素降解的微生物机制,依托红壤丘陵区长期定位试验,以两种土地利用方式(旱地和水旱轮作地)下两种施肥模式(化肥、秸秆还田配施化肥)的农田生态系统为研究对象,分析了表层土壤中纤维素含量、纤维二糖水解酶活性以及纤维素降解功能微生物丰度与群落结构的周年动态变化特征。结果表明:长期(13年)施肥后土壤中纤维素并未发生显著积累,且从周年动态变化来看,秸秆还田后旱地和水旱轮作地中纤维素分别在6个月和3个月内完全降解或被转化为其他形态;相关分析表明,纤维二糖水解酶活性与纤维素含量呈显著正相关,而真菌cbh I基因丰度与纤维二糖水解酶呈显著正相关(P0.01),因此功能基因cbh I可用于指示本研究供试土壤中降解纤维素的关键微生物群;聚类分析表明,旱地和水旱轮作地的纤维素降解微生物(含cbh I基因)互相分离,即与施肥相比,土地利用方式是引起土壤中纤维素降解微生物群落组成改变最主要的因素;克隆测序结果显示,两种土地利用方式下纤维素降解功能微生物均以伞菌和粪壳菌占绝对优势,分别占总克隆库的22.9%~39.5%(平均为34.7%)和17.7%~42.3%(平均为28.5%),其中秸秆还田后的纤维素降解过程可能由粪壳菌主导。研究结果阐明了红壤丘陵区旱地和水旱轮作地中秸秆还田后纤维素降解及其功能微生物群落的异同,为揭示农田土壤新鲜有机质中易分解组分(纤维素)的微生物转化机制提供了基础数据。

关 键 词:纤维素  旱地  水旱轮作地  纤维二糖水解酶  微生物群落
收稿时间:2017/4/5 0:00:00

Characteristics of cellulose-degrading microbial communities in upland and paddy-upland rotation land soils in red soil hilly region
WANG Yu-qing,CHEN Xiang-bi,DONG Ming-zhe,FENG Shu-zhen,HU Ya-jun,SU Yi-rong,GE Ti-d,ZHANG Zhen-hua and LI Qiao-yun.Characteristics of cellulose-degrading microbial communities in upland and paddy-upland rotation land soils in red soil hilly region[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2017,36(10):2071-2079.
Authors:WANG Yu-qing  CHEN Xiang-bi  DONG Ming-zhe  FENG Shu-zhen  HU Ya-jun  SU Yi-rong  GE Ti-d  ZHANG Zhen-hua and LI Qiao-yun
Institution:College of Biological Science and Technology, Hunan Agricultural University, Changsha 410128, China;The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China;Guangxi University of Science and Technology, Liuzhou 545006, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,The Key Laboratory of Subtropical Agro-Ecology, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125, China,Southern Regional Collaborative Innovation Center for Grain and Oil Crops in China, Hunan Agricultural University, Changsha 410128, China and College of Biological Science and Technology, Hunan Agricultural University, Changsha 410128, China
Abstract:Cellulose is the most abundant organic component in crop residue and thus plays a vital role in organic matter transformation in a gricultural soils. The degradation of cellulose in soil is mainly driven by microorganisms. The fungal cbhI gene is one of the key microbial genes participating in cellulose degradation. Based on long-term field experiments in subtropical hilly region, two land use types(upland and paddy-upland rotation land) and two fertilization treatments(chemical fertilizers and chemical fertilizers combined with crop straw) were selected for this study. The annual dynamics of cellulose content, cellobiohydrolase activity, and abundance and composition of cellulose-degrading microbial communities containing cbhI in surface soils were analyzed to reveal the characteristics of microbial decomposition of cellulose in agricultural soils. Results showed that after 13 years of long-term fertilization, cellulose had not accumulated significantly. Annual dynamic data indicated the newly added cellulose was degraded or converted into other forms within 6 and 3 months after straw incorporation into upland and paddy-upland rotation land soils, respectively. Both the Pearson correlation analysis and stepwise linear regression analysis showed that cellulose contents were positively related to the activity of cellobiohydrolase and that abundances of the fungal cbhI gene were positively related to cellobiohydrolase activity(P<0.01). This indicated that the fungal cbhI gene may be a potentially corresponding indicator of microbial decomposition of cellulose in the tested agricultural soils. Cluster analysis showed that cellulose-degrading microbial communities in upland soils and paddy-upland rotation land soils were separated from each other, suggesting that land-use type is the key factor in shaping cellulose-degrading microbial communities as compared with the fertilization treatments. Cloning and sequencing data showed that Agaricomycetes and Sordariomycetes, which accounted for 22.9%~39.5%(average 34.7%) and 17.7%~42.3%(average 28.5%) of total clones, respectively, were the dominant cellulolytic microbial groups. Sordariomycetes may dominate the microbial process of cellulose decomposition after crop straw returns to the field. This study clarified the similarities and differences of cellulose decomposition and its functional microbial communities between upland and paddy-upland rotation land after straw returns to the field, and thus provided the basic data on revealing microbial mechanisms of labile soil organic matter(cellulose) turnover in agricultural soils.
Keywords:cellulose  upland  upland-paddy rotation land  cellobiohydrolase  microbial community
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